The Structure of the Earth and Plate Tectonics

Transcription

1 The Structure of the Earth and Plate Tectonics

2 Agree or Disagree? 1. The Earth if made up of 4 different layers. 2. The crust (where we live) can be made of either less dense continental crust or the more dense oceanic crust. 3. There are 20 major plates that make up the crust. 4. These plates move around in all directions colliding, sliding past each other or are being forced apart. 5. Plates are made of rigid lithosphere. 6. The asthenosphere is above the lithosphere. 7. Circulations in the mantle cause crustal plates to move around and are called Convergence Cells.

3 The Formation of the Early Earth

4 Structure of the Earth The Earth is made up of 3 main layers: Core Mantle Crust Mantle Outer core Inner core Crust

5 The Crust This is where we live! The Earth s crust is made of: Continental Crust - thick (10-70km) - buoyant (less dense than oceanic crust) - mostly old Oceanic Crust - thin (~7 km) - dense (sinks under continental crust) - young

6 How do we know what the Earth is made of? Geophysical surveys: seismic, gravity, magnetics, electrical, geodesy Acquisition: land, air, sea and satellite Geological surveys: fieldwork, boreholes, mines

7 What is Plate Tectonics?

8 If you look at a map of the world, you may notice that some of the continents could fit together like pieces of a puzzle.

9 Plate Tectonics The Earth s crust is divided into 12 major plates which are moved in various directions. This plate motion causes them to collide, pull apart, or scrape against each other. Each type of interaction causes a characteristic set of Earth structures or tectonic features. The word, tectonic, refers to the deformation of the crust as a consequence of plate interaction.

10 World Plates

11 What are tectonic plates made of? Plates are made of rigid lithosphere. The lithosphere is made up of the crust and the upper part of the mantle.

12 What lies beneath the tectonic plates? Below the lithosphere (which makes up the tectonic plates) is the asthenosphere

13 Plate Movement Plates of lithosphere are moved around by the underlying hot mantle convection cells

14 Supercontinents! Practical Exercise 1 Read background information as a group. Follow the directions on the activity. Take about minutes with your neighbors to figure out the best way these land masses fit together. Be ready to discuss with the class your findings.

15 Agree or Disagree? 1. The Earth if made up of 4 different layers. 2. The crust (where we live) can be made of either less dense continental crust or the more dense oceanic crust. 3. There are 20 major plates that make up the crust. 4. These plates move around in all directions colliding, sliding past each other or are being forced apart. 5. Plates are made of rigid lithosphere. 6. The asthenosphere is above the lithosphere. 7. Circulations in the mantle cause crustal plates to move around and are called Convergence Cells.

16 What happens at tectonic plate boundaries?

17 Three types of plate boundary Divergent Convergent Transform

18 Divergent Boundaries Spreading ridges As plates move apart new material is erupted to fill the gap

19 Age of Oceanic Crust

20 Iceland: An example of continental rifting Iceland has a divergent plate boundary running through its middle

21 Convergent Boundaries There are three styles of convergent plate boundaries Continent-continent collision Continent-oceanic crust collision Ocean-ocean collision

22 Continent-Continent Collision Forms mountains, e.g. European Alps, Himalayas

23 Himalayas

24 Continent-Oceanic Crust Collision Called SUBDUCTION

25 Subduction Oceanic lithosphere subducts underneath the continental lithosphere Oceanic lithosphere heats and dehydrates as it subsides The melt rises forming volcanism E.g. The Andes

26 Ocean-Ocean Plate Collision When two oceanic plates collide, one runs over the other which causes it to sink into the mantle forming a subduction zone. The subducting plate is bent downward to form a very deep depression in the ocean floor called a trench. The worlds deepest parts of the ocean are found along trenches. E.g. The Mariana Trench is 11 km deep!

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28 Transform Boundaries Where plates slide past each other Above: View of the San Andreas transform fault

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30 How Far Will Your Plate Move Practical Exercise 2 Read background information as a group. Follow the directions on the activity. Take about minutes with your neighbors to figure out the best way these land masses fit together. Be ready to discuss with the class your findings.

31 Volcanoes and Plate Tectonics what s the connection?

32 Pacific Ring of Fire Volcanism is mostly focused at plate margins

33 Volcanoes are formed by: - Subduction - Rifting - Hotspots

34 Pacific Ring of Fire Hotspot volcanoes

35 What are Hotspot Volcanoes? Hot mantle plumes breaching the surface in the middle of a tectonic plate The Hawaiian island chain are examples of hotspot volcanoes. Photo: Tom Pfeiffer /

36 The tectonic plate moves over a fixed hotspot forming a chain of volcanoes. The volcanoes get younger from one end to the other.

37 Earthquakes and Plate Tectonics what s the connection?

38 As with volcanoes, earthquakes are not randomly distributed over the globe Figure showing the distribution of earthquakes around the globe At the boundaries between plates, friction causes them to stick together. When built up energy causes them to break, earthquakes occur.

39 Where do earthquakes form? Figure showing the tectonic setting of earthquakes

40 Plate Tectonics Summary The Earth is made up of 3 main layers (core, mantle, crust) On the surface of the Earth are tectonic plates that slowly move around the globe Plates are made of crust and upper mantle (lithosphere) There are 2 types of plate There are 3 types of plate boundaries Volcanoes and Earthquakes are closely linked to the margins of the tectonic plates